Sabi Sand Accommodation  South Africa, Big 5 Wildlife Safari at Luxury Lodges near Kruger Park South Africa
 

Sabie And Sand
Rivers Ecosystems

Arathusa Safari Lodge
Cheetah Plains Lodge
Chitwa Chitwa Game Lodge
Dulini Safari Lodge
Elephant Plains Game Lodge
Exeter Game Reserve
    - Kirkmans Kamp
    - Leadwood Lodge
    - River Lodge
Idube Private Game Reserve
Inyati Private Game Reserve
Leopard Hills Game Lodge
Lion Sands Game Reserve 
    - River Lodge
    - Ivory Lodge
    - 1933 Lodge
    - Tinga Lodge
    - Narina Lodge
Londolozi Game Reserve
    - Founders Camp
    - Private Granite Suites
    - Pioneer Camp
    - Tree Camp
    - Varty Camp
Mala Mala Game Reserve
    - Main Camp
    - Sable Camp
    - Rattray's on Mala Mala
Nkorho Bush Lodge
Nottens Bush Camp
Sabi Sabi Private Reserve
    - Bush Lodge
    - Earth Lodge
    - Little Bush Camp
    - Selati Camp
Savanna Pvt Game Reserve
Simbambili Game Lodge
Singita Game Reserve
    - Ebony Lodge
    - Boulders Lodge
    - Lebombo Lodge
    - Sweni Lodge
Ulusaba Safari Lodge
    - Cliff Lodge
    - Rock Lodge
    - Safari Lodge

Tours

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The accommodation in this domain is independently marketed by Far and Wild Safaris cc. We are an independent accommodation booking agency and Tour Operator marketing the Greater Sabie Sands Ecosystem area.
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Other Destinations
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Kruger Park
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Timbavati
Waterberg
Zululand

The escarpment and Malelane Mountains in the West and the Lebombo mountains in the East, were the most resistant to the forces of erosion by wind, rain and rivers. They therefore maintained a higher altitude than the rest of the Lowveld of the Sabi Sands biome.

Geology

The most ancient rocks are older that 3 500 million years. The most common of these are Granite/Gneiss with intrusions of Gabbro. As a result of a wet marshy period (about 300 - 200 million years ago), Ecca Shales were laid down on the Granite/Gneiss and Giabbro base.

The huge primitive Gondwanaland continent started breaking up about 200 million years ago. This break-up was caused by volcanic activity and tectonic movement. Molten rock burst through the crusts of the earth to form layers of Basalt. Further volcanic activity led to Rhyolite being laid down on top of the Basalt (about 180 million years ago). With the breaking up of Gondwanaland, the original flat beds of Granite/Gneiss, Ecca Shales, Basalt and Rhyolite split apart (about 135 million years ago). The eastern half of Southern Africa tilted towards the sea to the east. As the new continental edge and coastline of South East Africa developed, many of the present land-shapes and ecosystems of KNP had their beginning.

Altitude and Rainfall

Each Ecozone is an area with its own geology, rainfall, altitude and land-shape. The KNP is generally flat to undulating, with the central region averaging 260M above sea level. The only higher areas are the Lebombo Mountains in the east, the hills near Punda Maria in the north and the Malelane Mountains in the south. Khandzalive (near Malelane) is the highest point at 839M above sea level.

The KNP is a summer rainfall area (September to March), with an overall average of 500 mm per annum. The rain is often in the form of thunder-storms.

Rainfall generally decreases from the south to the north, and from the west to the east with Pafuri having the lowest average (40 mm p.a.). Pretoriuskop (740 mm p.a.) and Punda Maria (600 mm p.a.) are the highest rainfall areas.